By G. Shanmugam
This rock-based publication is an try to hyperlink deep-water method sedimentology with sandstone petroleum reservoirs. In featuring a constant procedure interpretation, the writer has depended on his description and interpretation of center and outcrop (1:20 to 1:50 scale) from 35 case stories (which comprise 32 petroleum reservoirs), totaling greater than 30,000 toes (9,145 m), conducted in past times 30 years (1974-2004). This booklet should still function a big resource of knowledge for college kids on historical past, method, first ideas, complex innovations, controversies, and useful purposes on deep-water sedimentology and petroleum geology * Discusses the hyperlink among deep-water approach sedimentology and petroleum geology * Addresses standards for spotting deposits of gravity-driven, thermohaline-driven, wind-driven, and tide-driven tactics in deep-water environments
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Additional info for Deep-Water Processes and Facies Models: Implications for Sandstone Petroleum Reservoirs
First deep-water field discovery (1968) in the Gulf of Mexico. ***System Type: TLP = Tension Leg Platform; FPS = Floating Production System. Blocks AC = Alaminos Canyon DC = DeSoto Canyon EB = East Breaks GB = Garden Banks GC = Green Canyon MC = Mississippi Canyon VK = Viosca Knoll History of deep-water research 27 Fig. 1. Types of deep-water development systems in the Gulf of Mexico. Fixed Platform (FP) is used for water depths up to 1500 ft (457 m). Compliant Tower (CT) is used for water depths between 1000 and 2000 ft (305–610 m).
Introduction and process sedimentology 17 (24) Quantify geological data (Sorby, 1908; Griffiths, 1960). Quantification is vital for demonstrating the relative importance of depositional processes through time (Fig. 9). 4 Interpretation (1) Interpret each bed in terms of the physics of the flow. Only through bed-bybed interpretation, an accurate quantification of facies can be made. (2) Apply James Hutton’s (1788) principle of Uniformitarianism (Chapter 6). Emphasize modern analogs for interpreting ancient systems.
However, it is not obvious from the graphic column the nature of grading trends. In contrast, a graphic lithologic column combined with expanded grain-size scale shows not only the nature of graded beds but also the exact position of graded bed contacts (Fig. 9). , depositional) sedimentary structures. , Pettijohn and Potter, 1964; Middleton, 1965; Middleton and Bouma, 1973; Middleton and Southard, 1977; Reineck and Singh, 1980; Allen, 1984; Collinson and Thompson, 1982; Harms et. , 1982). In addition to depositional structures, record post-depositional features.